Water cuts V-shaped valleys; glacierscarve out valleys that are U-shaped.
A round body of water formed by a glacier is known as a glacial lake. These lakes are created when glacial ice melts and fills depressions in the landscape. They can vary in size and depth and often have clear, cold water due to the sediment and minerals carried by the glacier. Glacial lakes are commonly found in mountainous regions and can be important for local ecosystems and water supplies.
Water cuts V-shaped valleys; glacierscarve out valleys that are U-shaped.-THIS IS TRUE.GRADPOINT/NOVANET ;) :) jesstyn wise ps3-jesstynwise ig-billgates217 fb-jesstyn wise
Misfit Stream
Glacial spillways are formed when meltwater from a retreating glacier creates a pathway through moraines or other glacial deposits. As the glacier retreats, the trapped water is released, carving out a channel that can carry large volumes of water downstream. These spillways are important for draining glacial lakes and preventing catastrophic flooding.
A glacial lake is typically a result of both erosion and deposition. Glacial erosion carves out depressions in the landscape, creating basins where water accumulates. Meanwhile, glacial deposition can form moraines or other features that dam up water and contribute to the formation of a glacial lake.
water cuts V-shaped valleys; glaciers carve out valley's that are U-shaped
Water cuts V-shaped valleys; glacierscarve out valleys that are U-shaped.-THIS IS TRUE.GRADPOINT/NOVANET ;) :) jesstyn wise ps3-jesstynwise ig-billgates217 fb-jesstyn wise
Lochs are formed by various geological processes, including glacial erosion, tectonic activity, or the accumulation of water in a basin. For example, glacial activity can carve out deep depressions that later become filled with water, creating a loch. The unique landscape of Scotland, for instance, is scattered with lochs that have been shaped by a combination of glaciation and other natural forces.
Valleys can be formed by various factors, including water erosion, glacial activity, and wind erosion. Water eroded valleys are typically created by rivers or streams, while glacial valleys are carved out by moving glaciers. Wind can also contribute to valley formation through processes like deflation or abrasion.
The channeled scablands formed through catastrophic flooding caused by the release of glacial lake water during the last ice age. The force of the water eroded the landscape, creating deep channels, steep-sided canyons, and large, flat-bottomed basins.
Most commonly, valleys are formed by water erosion, which can occur through processes such as river erosion and glacial erosion. Over time, flowing water can carve out valleys by gradually wearing away rocks and sediment, shaping the surrounding landscape.
Most large lakes in North America and Europe were likely formed by glacial activity during the last Ice Age. As glaciers advanced and retreated, they carved out depressions in the landscape, which later filled with water. Over time, these glacial lakes became some of the largest in the regions, including notable examples like the Great Lakes in North America. Additionally, post-glacial rebound and sedimentation further shaped the lakes we see today.